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Details

Autor(en) / Beteiligte
Titel
Influence of climatic teleconnections on the temporal isotopic variability as recorded in a firn core from the coastal Dronning Maud Land, East Antarctica
Ist Teil von
  • Journal of Earth System Science, 2010-02, Vol.119 (1), p.41-49
Ort / Verlag
India: Springer-Verlag
Erscheinungsjahr
2010
Link zum Volltext
Quelle
2022 ECC(Springer)
Beschreibungen/Notizen
  • Ice and firn core studies provide one of the most valuable tools for understanding the past climate change. In order to evaluate the temporal isotopic variability recorded in ice and its relevance to environmental changes, stable isotopes of oxygen and hydrogen were studied in a firn core from coastal Dronning Maud Land, East Antarctica. The annual δ 18 O profile of the core shows a close relation to the El Niño Southern Oscillation (ENSO) variability. The ENSO indices show significant correlation with the surface air temperatures and δ 18 O values of this region during the austral summer season and support an additional influence related to the Southern Annular Mode (SAM). The correlation between the combined ENSO-SAM index and the summer δ 18 O record seems to have been caused through an atmospheric mechanism. Snow accumulation in this region illustrates a decreasing trend with opposite relationships with δ 18 O data and surface air temperature prior and subsequent to the year 1997. A reorganization of the local water cycle is further indicated by the deuterium excess data showing a shift around 1997, consistent with a change in evaporation conditions. The present study thus illustrates the utility of ice-core studies in the reconstruction of past climate change and suggests possible influence of climatic teleconnections on the snow accumulation rates and isotopic profiles of snow in the coastal regions of east Antarctica.
Sprache
Englisch
Identifikatoren
ISSN: 0253-4126, 2347-4327
eISSN: 0973-774X
DOI: 10.1007/s12040-010-0006-9
Titel-ID: cdi_proquest_miscellaneous_746272085

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